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Volume 20 Number 2
  • E-ISSN: 1365-2478

Abstract

A

A method is presented for determining the lower surface of a two‐dimensional body producing a magnetic anomaly when its upper surface and the intensity of magnetization are given. The magnetization vector is assumed to lie along a specified direction but the sense of magnetization may be different in different vertical sections of the body and may be regarded as unknown. The method is illustrated using the computed anomalies of some theoretical models.

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/content/journals/10.1111/j.1365-2478.1972.tb00646.x
2006-04-27
2024-04-20

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References

  1. Al‐Chalabi, M., 1970, Interpretation of two‐dimensional magnetic profiles by non‐linear optimisation. Bollettino di Geophysica Teorica ed Applicata3–19.
  2. Bott, M. H. P., and Hutton, M. A., 1970, Limitations on the resolution possible in the direct interpretation of marine magnetic anomalies. Earth and Planetary Science letters8, 317–319.
    [Google Scholar]
  3. Johnson, W. W., 1969, A least squares method of interpreting magnetic anomalies caused by two‐dimensional structures. Geophysics34, 65–74.
    [Google Scholar]
  4. Kunaratnam, K., 1963, Applications of Digital Electronic Computers to gravity and magnetic interpretation. Ph. D. Thesis, University of London.
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  • Article Type: Research Article

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